Invertebrados marinos del Devónico inferior de la Formación Lolén, Sierra de la Ventana, Provincia de Buenos Aires

SICCARDI, ARÓN; URIZ, NORBERTO JAVIER; CINGOLANI, CARLOS ALBERTO; RUSTÁN, JUAN JOSÉ

General Roca, Río Negro

Jornada; Jornadas de Comunicaciones de la Asoc. Paleont. Argentina; 2012

The Ventania System is located in the south-western Buenos Aires province, Argentina and is classically correlated to units of similar age outcropping in the Malvinas Islands, the Cape Fold Belt (South Af r ica) and El lswor th Mountains (Antarctica). It is characterized by an intense folding of the entire Paleozoic siliciclastic sedimentary record. Three sedimentary units are known as Curamalal, Ventana and Pillahuincó Groups. The Ventana Group (1300 m thick) is part of a Middle Ordovician-Middle Devonian marine siliciclastic sedimentary sucession and is unconformably overlain by diamictites of the Pennsylvanian Gondwanan glaciations. Four lithostratigraphic units have been recognized within the Ventana Group, from base to top: Bravard, Napostá, Providencia and Lolén. The Lolén Formation is mainly composed of feldspatic sandstones, wackes, and interbedded black shales, with shallow marine sedimentary structures. The lower section of the Lolén Formation records marine invertebrates (mainly brachiopods and bivalves) preserved in sandy levels corresponding to supratidal to subtidal depositional environments. New records include the brachiopods Proboscidina  I s a a c s o n , 1 9 7 7 , Scaphiocoelia? Whitfield, 1891, and a Muttationellid indet., bivalves like Nuculidae?, Mallettidae and Nuculanidae?, some gastropods (Plectonotus? sp Clarke, 1899) and abundant trace fossils. The p r e s e n c e o f P r o b o s c i d i n a a n d Scaphiocoelia? suggest an age not younger than Emsian for the bearing layers, although (taking into account the stratigraphic rank of Scaphiocoelia? In Bolivian strata) a Pragian age should not be excluded. Hence, previous interpretations on the Early Devonian age of the lower part of the Lolén Formation in Eastern Argentina are supported by the new paleontological evidence.